河漫灘沉積 的英文怎麼說

中文拼音 [màntānchén]
河漫灘沉積 英文
flood-plain deposit
  • : 1 (天然的和人工的大水道) river 2 (指銀河系) the milky way system; the galaxy 3 (特指黃河) t...
  • : Ⅰ動詞(水滿外流) overflow; flood; brim over; inundate Ⅱ形容詞1 (到處都是; 遍) all over the pla...
  • : 名詞1. (岸邊) beach; sands 2. (江河中水淺多石而水流湍急處) rapids; shoal
  • : Ⅰ動詞1 (沉沒; 墜落) sink 2 (沉下 多指抽象事物) keep down; lower 3 [方言] (停止) rest Ⅱ形容...
  • : Ⅰ動詞(積累) amass; store up; accumulate Ⅱ形容詞(長時間積累下來的) long standing; long pending...
  • 沉積 : [地] deposit; sedimentation; deposition; precipitation
  1. Because during the sedimentation of the flood plain - estuary fades, the conditions of sea level rising, tidal regime, sediment supply and accommodation space were suitable for the development of a tidal ridge system, the sand lenses associated with this facies may represent tidal ridge formation in the incised valley

    口灣相期問,由於海平面上升、潮流體系、物供給和可容空間條件適合一個潮流沙脊體系的發育,其中的砂質透鏡體可能代表了下切谷內發育的潮流沙脊。
  2. Then it makes a summary of the terrestrial carbon deposition and points out several potential land - origin carbon traces including dam capture, deposition happening in floodplain, estuary and near - shore area, and terrestrial carbon precipitation

    之後對陸地碳機制進行了歸納,指出了包括大壩截留,口近岸帶及陸地碳降等幾種可能的陸源碳蹤跡。
  3. Those within existing stream channels are much less stable than overbank deposits.

    現在槽內物的穩定性比物差的多。
  4. The comparison of the component particles of baijiaziu profile and mafangtan profile with that of modern flood plain substance of weihe river indicates that the river impetus of weihe river has gradually been getting weaker, which reveals that it has gradually been getting dryer since the last 1300 years

    西安高陵白家嘴物粒度隨深度的變化及其與渭現代河漫灘沉積物粒度特徵的對比表明,渭近1 3ha來有流量減少,流速減慢,水深變淺的發展趨勢。
  5. At the end of late pleitocene, influenced by the climate of glacier period, the last great event of the region in the geological time was taken place so that the migration and extinction of organism species were resulted, loess accumulation was generally developed throughout the whole region, in the holocene, the most important environmental change was fluvial process, which was still influnced by two factors - neotectonics and palaeoclimatic changes

    更新世晚期末,受末次冰期氣侯的影響,本區發生了地史時期的最後一次大事件,造成了物種遷移和絕滅,全區廣泛發育黃土堆。進入全新世,本區環境變化以流作用最為顯著,物主要分佈在各大水系的谷中,構成一、二級階地和近代床與
  6. The sediments of the incised valleys show an upward - fining succession, and can be grouped into four sedimentary fades : gravel lag - deposit of in - channel to partly over bank sediments of a meandering river, flood plain - estuary, estuary - shallow marine, and estuary sand bar, based on lithology, paleontology, and sedimentary textures and structures

    根據巖石學、結構和構造特徵,本區下切谷充填物具有向上變細的層序,可以劃分為4個相類型:床滯留物到部分曲流體系的邊口灣口灣淺海口灣砂壩
  7. The seawater thereafter withdrawed southward away from the area, and form abundant stream, lake and delta deposit in shanxi stage and the early shihezi stage and stream, lake and bog deposit in the late shihezi stage and shiqianfeng stage

    隨后,海水向南退出本區,並在山西期、石盒子早期形成廣泛的流、湖泊和三角洲,在石盒子晚期和石千峰期形成流、湖泊和沼澤
  8. The researches of dynamic behavior and liquefaction potential of saturated sands have been further. however, more and more macroscopic liquefaction phenomena and experimental investigations show that different depositional environments lead to different structure of soils, while the influence of structure property of soils on liquefaction resistance is no less than that of density and consolidation stress and so on. ancient alluvial flat deposits, namely recently deposited soils, are easier liquefaction during earthquake

    對於一般飽和砂土的動力特性和液化勢的研究已比較深入,然而,愈益增多的宏觀現象和試驗研究表明,由於土的環境不同而導致土的結構性的差異,而土的結構性對抗液化能力的影響並不亞於密度、固結壓力等因素,古物即新近土在地震當中更容易液化。
  9. Alluvial soil a type of soil formed on river floodplains and deltas, where new sediment is deposited on the land during floods

    土:在和三角洲地帶由洪水沖刷泥沙而形成的土壤類型。
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